Comparing IRI and regional ionospheric model with ionosonde foF2 measurements in Pakistan

Critical frequency of F2 layer acquired by three ionosonde stations, Karachi (KHI, 24.95°N, 67.13°E), Multan (MUL, 30.18°N, 71.48°E) & Islamabad (ISL, 33.75°N, 73.13°E), in Pakistan has been compared with foF2 obtained from global ionospheric model IRI-2012 and computed from regional ionospheric model using higher terms of Emperical Orthogonal Functions (EOFs) during summer (July). The data has been compared at different phases of solar epoches. The computational sets using higher number of terms of EOFs (L > 1) showed slight different deviations from observations with respect to the expansion of EOFs using least number of terms (L = 1). Both models revealed good to reasonable agreement with the observed values for Multan and Islamabad. However for Karachi, considerable deviations between the models and observations are noted at different solar epoches except deep solar minimum due to its location which lies within equatorial ionization anomaly region. In general, regional model gives better results compared to IRI for MUL and ISL whereas IRI worked better for Karachi. Thus further improvements in regional model are required to get promosing results especially for EIA region station.

[1]  A. Ridley,et al.  Modeling ionospheric foF2 by using empirical orthogonal function analysis , 2011 .

[2]  J. Forbes,et al.  Principal modes of thermospheric density variability: Empirical orthogonal function analysis of CHAMP 2001–2008 data , 2010 .

[3]  M. Ayub,et al.  Study of maximum electron density NmF2 at Karachi and Islamabad during solar minimum (1996) and solar maximum (2000) and its comparison with IRI , 2009 .

[4]  D. Bilitza,et al.  International Reference Ionosphere 2007: Improvements and new parameters , 2008 .

[5]  Ghulam Murtaza,et al.  Comparing IRI and a regional model with ionosonde measurements in Pakistan , 2008 .

[6]  Biqiang Zhao,et al.  An empirical orthogonal function model of total electron content over China , 2008 .

[7]  W. Wan,et al.  Modeling M(3000)F2 based on empirical orthogonal function analysis method , 2008 .

[8]  C. Mitchell,et al.  Imaging of the equatorial ionospheric anomaly over South America—A simulation study of total electron content , 2006 .

[9]  P. Fagundes,et al.  IRI-2001 model predictions compared with ionospheric data observed at Brazilian low latitude stations , 2006 .

[10]  Biqiang Zhao,et al.  Statistical characteristics of the total ion density in the topside ionosphere during the period 1996-2004 using empirical orthogonal function (EOF) analysis , 2005 .

[11]  Daniel R. Marsh,et al.  An empirical model of nitric oxide in the lower thermosphere , 2003 .

[12]  Z. Khan,et al.  On the cause of fore-noon & post-noon bite-outs in foF2 , 1985 .

[13]  W. Wan,et al.  An Empirical Orthogonal Function (EOF) Analysis of Ionospheric Electron Density Profiles Based on the Observation of Incoherent Scatter Radar at Millstone Hill , 2008 .

[14]  N. I. Dvinskikh,et al.  An adaptable regional empirical ionospheric model , 1991 .

[15]  N. I. Dvinskikh Expansion of ionospheric characteristics fields in empirical orthogonal functions , 1988 .